A dyke and a sill are both types of igneous intrusions, but they differ in their orientation and formation. A dyke is a vertical or steeply inclined intrusion that cuts across the existing rock layers, while a sill is a horizontal or near-horizontal intrusion that lies parallel to the existing rock layers. Dykes typically form from magma that rises through fractures, whereas sills form when magma intrudes between layers of rock. Their differing orientations influence the geological features and structures they create.
Dyke Baronets was created in 1677.
Garth Dyke was born in 1971.
Two, Dick Van Dyke and Barry Van Dyke.
Barry Van Dyke's birth name is Barry Wayne Van Dyke.
Michael Van Dyke's birth name is Michael John Van Dyke.
If vertical, a dyke; if horizontal, a sill.
A Sill is formed when a fluid rock (usually magma but it can be mud or salt) is squeezed in between the layers (usually horizontal) of older rocks before it solidifies in place. A Dike or Dyke is the opposite, here the fluid rock penetrates across the layering of the older rocks. Logically to get the material to form a Sill there must be an accompanying feeder Dyke.
Both of these are called igneous intrusions. They form when liquid magma forces its way into cracks in existing rocks and sets. If the resulting band of rock is basically vertical it is called a dyke, and if it is more horizontal it is a sill.
dyke - verticall lava through a rock. sill - horizontall lava through a rock. pillow lavas - pillows sold in asda which support your gullable head as you sleep.
From your statement it sounds like you are referring to an igneous dyke rather than a sill, however see the following: A sill is a sheet of intruded magma that forms between to layers of older "country" rock. This is technically described as a "concordant sheet intrusion". If it is later over turned due to tectonic folding it may be vertical but as it was originally emplaced between and parallel to pre-existing rock layers, it is still an igneous sill! However if the intrusion cross cuts the bedding planes of the country rock - known as a discordant intrusion (and was originally (sub)vertical at the time of emplacement) it is known as a dyke. For more information please see the related link.
Judee Sill's birth name is Judith Lynn Sill.
Intrusions occur when magma cuts through weaknesses in rock layers and forms a band of igneous rock. Sometimes the new band is approximately horizontal and it is called a sill. If it is more vertical it is called a dyke.
Rachel is a dyke. Guess who?? Haha Rachel is a dyke. Guess who?? Haha Rachel is a dyke. Guess who?? Haha Rachel is a dyke. Guess who?? Haha Rachel is a dyke. Guess who?? Haha Rachel is a dyke. Guess who?? Haha
sill opening of a wall
The bird landed on the window sill
Dyke = Deich
The small flat area of a window is a window sill. I place plants on my window sill.